GOTM as a host for interstitial water / sea-floor / sediment? #80
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lumlauf
platipodium
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Hi Carsten,
Are you aware that we recently extended GOTM to include a vertically
resolved sediment module in GOTM (see
https://doi.org/10.1029/2023JC019651
<https://doi.org/10.1029/2023JC019651>)? At the moment, benthic
transports are exclusively diffusive (cohesive sediments). But we are
working on an extension towards non-cohesive sediments with advective
fluxes, driven by surface-wave effects. Is this what you mean when
talking about interstitial water?
…-Lars
On 12/17/2025 9:26 AM, Carsten Lemmen wrote:
I am aware that GOTM is all about turbulence and so running it in a
non-turbulent environment, like in interstitial water within a
sediment might miss its strength. But could still provide its rich
infrastructure (flexout, fabm, B.C) !!
Let me still ask: is it possible to parameterise GOTM such that it
runs in interstitial water?
This would probably require adding some information on porosity
(possibly as a profile, or get around this with some other hack) and
it would mean to reduce turbulence and diffusivity a lot.
But maybe this is a stupid idea?
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------------------------------------------------
Lars Umlauf
Department of Physical Oceanography
Leibniz-Institute for Baltic Sea Research
phone : ++49 381 5197 223
fax : ++49 381 5197 114
web :www.io-warnemuende.de/lars-umlauf-en.html
address:
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Germany
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Answer selected by
platipodium
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Hi Carsten,
We actually have an improved, more recent version of this code, which
has been carefully tested and is also now based on the most recent
version of FABM. I'll send you a separate email with all the relevant
people in CC in a minute.
Cheers,
Lars
…On 12/17/2025 6:17 PM, Carsten Lemmen wrote:
HI Lars, this is /exactly/ what I was looking for! And no, I was not
aware of the publication, thanks for pointing me to it. I'll try to
replicate the work with the setups claimed to be published on
Zenodo... anything else I need to be aware of?
Thanks,
Carsten
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------------------------------------------------
Lars Umlauf
Department of Physical Oceanography
Leibniz-Institute for Baltic Sea Research
phone : ++49 381 5197 223
fax : ++49 381 5197 114
web :www.io-warnemuende.de/lars-umlauf-en.html
address:
Leibniz-Institute for Baltic Sea Research
Seestrasse 15
D-18119 Rostock-Warnemuende
Germany
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Is it an FABM only thing - or changes to GOTM as well? |
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As far as I understand, only/mainly the interface to FABM has been
modified. Strongly modified as it now also includes the grid, variables,
and time stepping for the vertically resolved sediment compartment.
But Knut would be the better person to comment on this. He has
implemented it.
Lars
…On 12/17/2025 7:25 PM, Karsten Bolding wrote:
Is it an FABM only thing - or changes to GOTM as well?
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------------------------------------------------
Lars Umlauf
Department of Physical Oceanography
Leibniz-Institute for Baltic Sea Research
phone : ++49 381 5197 223
fax : ++49 381 5197 114
web :www.io-warnemuende.de/lars-umlauf-en.html
address:
Leibniz-Institute for Baltic Sea Research
Seestrasse 15
D-18119 Rostock-Warnemuende
Germany
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I am aware that GOTM is all about turbulence and so running it in a non-turbulent environment, like in interstitial water within a sediment might miss its strength. But could still provide its rich infrastructure (flexout, fabm, B.C) !!
Let me still ask: is it possible to parameterise GOTM such that it runs in interstitial water?
This would probably require adding some information on porosity (possibly as a profile, or get around this with some other hack) and it would mean to reduce turbulence and diffusivity a lot.
But maybe this is a stupid idea?
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